基于热成像的土壤性质二维评价

C. Nakayama, T. Katsumata, H. Aizawa, S. Komuro, H. Arima
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引用次数: 0

摘要

采用脉冲加热技术对火山灰土的主要成分之一土样的温度响应进行了测量。利用二维辐射测温仪和热电偶对不同试样的温度响应进行了含水量计算。红外辐射测温是一种非接触式、非破坏性的从材料表面温度变化来检测材料性质或内部状况的技术。用由两个衰减分量组成的指数曲线计算了表面温度的衰减寿命。利用热图像评估了快速组分的二维分布。利用热成像计算出的快速衰减组分的寿命,可以评估含水量的二维分布。土壤的动态特性对农业土壤的评价具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Two-dimensional evaluation of soil property based on thermal imaging
Temperature response of soil specimens, which is one of major contains of volcanic ash soil, are measured by pulse heating technique. Water contents of various specimens are evaluated from temperature response of specimens using two-dimensional radiation thermometer and thermocouples. Infrared radiation thermometry is a non-contact and non-destructive technique to detect the properties or internal conditions of a material from the temperature variation of surface. Decay lifetime of surface temperature is calculated with exponential curve composed from two decay components. Two-dimensional distribution of faster component dasiatau1psila is evaluated with using thermal images. Two-dimensional distribution of water contents can be evaluated using lifetime of faster decay components calculated from thermal imaging. Dynamic characteristics of soil are suggested to be useful for evaluation of soil for agriculture.
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